Quantum chemical modelling at the atomic level led to the realisation of how phosphate binding to iron minerals depends on pH, the structure of the phosphate compounds and the coverage of the minerals with organic molecules. Practical instructions for action include controlling the pH value by liming and the humus content by increasing the supply of organic residues in order to minimise P fixation. At the molecular level, new insights were gained into the genes that control P utilisation in soil microorganisms and plants. Of the relevant groups of bacteria, those that are naturally associated in the soil with intercropping plants suitable for cultivation (e.g. Bradyrhizobiacae on Serradella) or that are suitable as authorised strains for the development of inoculants for P recycling products (e.g. Bacillus velezensis) are to be promoted. Such P-recycling products, e.g. biochars from P-rich materials such as bones and sewage sludge, have been tested in a variety of experimental approaches. The results consistently showed that, for example, a bone char loaded with sulphur had a similarly good fertilising effect as the commercial fertiliser tripel superphosphate. Several years of plot and field trials with bone char and biochar from sewage sludge led to the same result. The in-depth evaluation of P fertilisation trials in Germany and the EU led to the conclusion that the importance of P fertilisation for yield levels was probably significantly overestimated in the past.
The recommended P fertilisation did not always lead to higher yields in all soil P content classes. Even after suspending P fertilisation for 36 years, significant reductions in yield were only observed for sugar beet, but not for winter cereals. It follows that a more economical use of P fertilisers makes economic and ecological sense. Investigations of P discharge in drained lowland catchment areas led to the realisation that discharges with the base flow are negligible.
In contrast, heavy rainfall events lead to peaks in runoff and P discharges. This can be explained by erosion, superficial and ‘internal’ discharges in the soil profile. Avoiding such runoff peaks is extremely challenging and has not yet been satisfactorily solved technically. Therefore, the limitation of agricultural P inputs remains The same result was achieved in several years of plot and field trials with bone char and biochar from sewage sludge. The in-depth evaluation of P fertilisation trials in Germany and the EU led to the conclusion that the importance of P fertilisation for yield levels was probably significantly overestimated in the past.